DOCSLIB.ORG

Rockaway Resiliency Projects & Fema Funding

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Rockaway Resiliency Projects & Fema Funding ROCKAWAY RESILIENCY PROJECTS & FEMA FUNDING PS/MS 42 Robert Vernam School December 12, 2016 TONIGHT’S MEETING . Anticipate excess Rockaway Boardwalk funds . Mayoral commitment to use funds for resiliency projects in Rockaways . Submitted Alternate Projects need to be approved by FEMA prior to the completion of Rockaway boardwalk (Anticipated completion date is Memorial Day 2017) TONIGHT . Present potential projects . Get your feedback! 2 ROCKAWAYS RECOVERY & RESILIENCY INVESTMENTS 3 PROPOSED USACE ROCKAWAY REFORMULATION 4 FEMA SECTION 428 PILOT PROGRAM . The FEMA 428 program allows for anticipated savings from a FEMA 428 project to be applied to Alternate Projects . NYS and FEMA determines eligibility of projects and approves use of underrun funding FEMA ELIGIBILITY ELIGIBLE NOT ELIGIBLE . Raised Shoreline Work . Landscaping projects: . Parks and Recreational . New Trees Facilities . Plantings . Buildings . Lawns . Elevation of Structures . Buyouts . Engineered Natural . Studies Structures 5 PROJECT CONSIDERATIONS Projects build off existing studies: . HPD Resilient Edgemere Initiative . Rockaway Parks Conceptual Plan Project Considerations: Resiliency . Protect neighborhoods from tidal flooding . Environmental restoration . Improve access/activate waterfront Recovery . Restore/replace facilities directly lost during Hurricane Sandy Community . Provide recreational or community CONSIDERATIONS amenities/priorities Does not meet Public Feedback Partially meets Fully meets 6 PROJECT SOURCE Rockaway Parks Conceptual Plan Resilient Edgemere Plan NYC Parks Projects presented geographically east to west 7 PROJECT #1 BAYSWATER PARK Renovate community park $50M - $60M Projects presented geographically east to west 8 PROJECT #1 BAYSWATER PARK Existing Bayswater Park Resiliency Recovery Community 9 PROJECT #1 BAYSWATER PARK Resiliency Features: . Raised Berm with Trail . Permeable Pavement . Stormwater Retention . Shoreline Bank Stabilization . Wetland and Coastal Forest Restoration Resiliency Recovery Community 10 PROJECT #1 BAYSWATER PARK Community Features: . Athletic Fields . Running Track . Play Area . Kayak Launch . Water Feature . Refurbished Comfort Station . Public Plaza . Sport Courts Resiliency Recovery Community 11 PROJECT #2 RAISE SHORELINES EDGEMERE Protection against sea level rise and tidal flooding $20M - $30M Projects presented geographically east to west 12 PROJECT #2 RAISE SHORELINES EDGEMERE Flooding in Edgemere (February 2016) Resiliency Recovery Community 13 PROJECT #2 RAISE SHORELINES EDGEMERE Resiliency Features: . Vegetated berm along perimeter of peninsula . New bulkhead at northern tip of peninsula . Drainage study to address nuisance flooding Community Benefit: . Reduced flooding nuisance Resiliency Recovery Community 14 PROJECT #3 ROCKAWAY COMMUNITY PARK Renovate community park $40M - $50M Projects presented geographically east to west 15 PROJECT #3 ROCKAWAY COMMUNITY PARK Existing Rockaway Community Park Resiliency Recovery Community 16 PROJECT #3 ROCKAWAY COMMUNITY PARK Resiliency Features: . Raised berm along west & east edges of park . Shoreline Bank Stabilization . Wetland Restoration Ocean Bay Apartments Resiliency Recovery Community 17 PROJECT #3 ROCKAWAY COMMUNITY PARK Community Features: . Athletic Fields . Game Tables . Skate Park . Kayak Launch . Picnic Area . Sport Courts . Comfort Station Resiliency Recovery Community 18 PROJECT #4 THURSBY BASIN PARK Create new waterfront park $20M - $30M Projects presented geographically east to west 19 PROJECT #4 THURSBY BASIN PARK Existing Thursby Basin Park Site Resiliency Recovery Community 20 PROJECT #4 THURSBY BASIN PARK Resiliency Features: . Seawall/raised berm . Rain Garden . Waterfront Plantings Resiliency Recovery Community 21 PROJECT #4 THURSBY BASIN PARK Community Features: . Sports Courts . Play Area . Water Feature . Kayak Launch Resiliency Recovery Community 22 PROJECT #5 ROCKAWAY OPERATIONS HQ Reconstruct Parks’ maintenance and operations facility $20M - $30M Projects presented geographically east to west 23 PROJECT #5 ROCKAWAY OPERATIONS HQ Resiliency Recovery Community 24 PROJECT #5 ROCKAWAY OPERATIONS HQ Hurricane Sandy Water Line Community Benefits: . Services over 130 parks properties in Rockaways and Broad Channel . Provides emergency response services during storm season Resiliency Recovery Community 25 PROJECT #5 ROCKAWAY OPERATIONS HQ Resiliency/Recovery Features: . Reconstruct and elevate whole facility Resiliency Recovery Community 26 PROJECT #6 BEACH 88TH STREET PARK Create new waterfront park $40M - $50M Projects presented geographically east to west 27 PROJECT #6 BEACH 88TH STREET PARK Existing Beach 88th Street Park Site Resiliency Recovery Community 28 PROJECT #6 BEACH 88TH STREET PARK Resiliency Features: . Seawall/raised berm . Invasive Species Removal . Wetland Restoration . Native Plant Introduction Resiliency Recovery Community 29 PROJECT #6 BEACH 88TH STREET PARK Community Features: . Comfort Station . Kayak Dock . Shade Structure . Picnic Seating . Play Area Resiliency Recovery Community 30 PROJECT #7 BEACH 94TH – 95TH CORRIDOR Gateway corridor to Rockaways $20M - $30M Projects presented geographically east to west 31 PROJECT #7 BEACH 94TH - 95TH CORRIDOR Existing Parking Area Resiliency Recovery Community 32 PROJECT #7 BEACH 94TH - 95TH CORRIDOR Resiliency Features: . Permeable Pavement . Bioswales to Absorb Stormwater . New Street Trees Community Uses: . Markets . Festivals/Events . Café Seating Resiliency Recovery Community 33 PROJECT #8 SHORE FRONT PARKWAY REC ZONE Rebuild recreation areas $20M - $30M Projects presented geographically east to west 34 PROJECT #8 SHORE FRONT PARKWAY REC ZONE Existing Shore Front Parkway Resiliency Recovery Community 35 PROJECT #8 SHORE FRONT PARKWAY REC ZONE Recently Completed Roller Hockey Rink Resiliency Recovery Community 36 PROJECT #8 SHORE FRONT PARKWAY REC ZONE Recovery & Community Amenities: . Performance Space . Dog Run . Multi-Purpose Athletic Field . Playground with Water Feature . Rock Climbing & Adventure Course . Labyrinth and Seating Area Resiliency Recovery Community 37 PROJECT #8 SHORE FRONT PARKWAY REC ZONE Example of Multi-Purpose Athletic Field Example of Rock Climbing Structure Resiliency Recovery Community 38 PROJECT #9 SHORE FRONT COMFORT STATIONS Build new comfort stations at Beach 116th and Beach 59th $30M - $40M Projects presented geographically east to west 39 PROJECT #9 SHORE FRONT COMFORT STATIONS Resiliency Features: . Buildings and utilities elevated to 500-year flood plain Resiliency Recovery Community 40 PROJECT #9 SHORE FRONT COMFORT STATIONS Decommissioned Below-Ground Beach 116th Street Comfort Station Resiliency Recovery Community 41 NEXT STEPS . Incorporate Community Feedback . Submit to FEMA . FEMA Approval . Secure Additional Funds . Project design QUESTIONS? 42 Please submit comments and ideas to [email protected] by December 20th, 2016. THANK YOU! 43.
Load more

Recommended publications
  • Post-Glacial Sea-Level Change Along the Pacific Coast of North America Dan H
    University of Washington Tacoma UW Tacoma Digital Commons SIAS Faculty Publications School of Interdisciplinary Arts and Sciences 8-1-2014 Post-glacial sea-level change along the Pacific coast of North America Dan H. Shugar University of Washington Tacoma, [email protected] Ian J. Walker Olav B. Lian Jordan BR Eamer Christina Neudorf See next page for additional authors Follow this and additional works at: https://digitalcommons.tacoma.uw.edu/ias_pub Recommended Citation Shugar, Dan H.; Walker, Ian J.; Lian, Olav B.; Eamer, Jordan BR; Neudorf, Christina; McLaren, Duncan; and Fedje, Daryl, "Post-glacial sea-level change along the Pacific oc ast of North America" (2014). SIAS Faculty Publications. 339. https://digitalcommons.tacoma.uw.edu/ias_pub/339 This Article is brought to you for free and open access by the School of Interdisciplinary Arts and Sciences at UW Tacoma Digital Commons. It has been accepted for inclusion in SIAS Faculty Publications by an authorized administrator of UW Tacoma Digital Commons. Authors Dan H. Shugar, Ian J. Walker, Olav B. Lian, Jordan BR Eamer, Christina Neudorf, Duncan McLaren, and Daryl Fedje This article is available at UW Tacoma Digital Commons: https://digitalcommons.tacoma.uw.edu/ias_pub/339 1 Post-glacial sea-level change along the Pacific coast of North 2 America 3 Dan H. Shugar1,*, Ian J. Walker1, Olav B. Lian2, Jordan B.R. Eamer1, Christina 4 Neudorf2,4, Duncan McLaren3,4, Daryl Fedje3,4 5 6 1Coastal Erosion & Dune Dynamics Laboratory, Department of Geography, 7 University of Victoria, Victoria, BC,
    [Show full text]
  • Glaciomarine Deltas of Maine and Their Relation to Late Pleistocene-Holocene Crustal Movements
    Maine Geological Survey Neotcctonics of Maine 1989 Glaciomarine Deltas of Maine and Their Relation to Late Pleistocene-Holocene Crustal Movements Woodrow B. Thompson Maine Geological Survey Augusta, Maine 04333 Kristine J . Crossen Geology Department University ofAlaska Anchorage, Alaska 99507 Harold W. Borns, Jr. Institute for Quaternary Studies University of Maine Orono, Maine 04469 Bjorn G. Andersen University of Oslo Oslo, Norway ABSTRACT The deglaciation of southern Maine in late Wisconsinan time was accompanied by marine submergence of the isostatically-depressed coastal lowland. Glacial meltwater streams deposited over 100 Gilbert-type deltas into the sea during the transgressive phase of submergence, between about 14,000 and 13,000 yr B.P. These deltas were deposited either in contact with the ice margin or very close to it. They are classified into four categories based on depositional environment: ice-contact deltas (39% ), esker-fed ice-contact deltas (30% ), leeside deltas (26% ), and distal outwash deltas (5% ). Most of the deltas for which subsurface data are available accumulated in water less than 80 m deep, and the ice-contact deltas are believed to have formed along a grounded tidewater-glacier margin. Bedrock strike ridges and other hills slowed the retreat of the ice margin, causing brief stillstands during which deltas were deposited adjacent to these topographic highs. The sequence of glaciomarine deltas in Maine probably formed when the transgressing sea had reached its maximum depth and relative sea level was beginning to fall in response to isostatic crustal uplift. The elevations of the contacts between the topset and foreset beds of 65 deltas in Maine and New Brunswick were measured in order to locate the positions of sea level to which the deltas were graded.
    [Show full text]
  • Raised Shoreline Phenomena and Postglacial Emergence in South
    Document généré le 26 sept. 2021 07:54 Géographie physique et Quaternaire Raised Shoreline Phenomena and Postglacial Emergence in South-Central Newfoundland Les lignes de rivage soulevées et l'émersion postglaciaire au centre-sud de Terre-Neuve Вoзвышeнный peльeф пoбepeжья и пocлeлeдникoвый пpиpocт cуши нa южном подерeжьe цeнтpaльнoгo Hьюфaундлeндa C. M. Tucker, D. A. Leckie et S. B. McCann Volume 36, numéro 1-2, 1982 Résumé de l'article Dans la région de Burin-Hermitage, au sud de Terre-Neuve, on retrouve deux URI : https://id.erudit.org/iderudit/032475ar types de lignes de rivage marines soulevées: des plates-formes marines DOI : https://doi.org/10.7202/032475ar entaillées dans la roche en place ainsi que des terrasses et des plages développées dans des matériaux meubles. La plupart des plates-formes datent Aller au sommaire du numéro d'avant le Wisconsinien inférieur. Une ligne de rivage rocheuse horizontale située à 4,5 ± 1,5 m, qu'on retrouve à travers la région, fut probablement formée au cours du dernier interglaciaire. Des deltas soulevés et des épandages Éditeur(s) fluvioglaciaires côtiers, associés à des plans d'eau marins qui marquent la limite marine du Wisconsinien inférieur dans la partie nord de la zone d'étude, Les Presses de l'Université de Montréal sont mis en relation avec des terrasses et des plages soulevées existant plus au sud dans la péninsule de Burin. L'altitude de ces formes sert à établir le mode ISSN régional d'émersion post-glaciaire. Il s'est produit une emersion de plus de 30 m dans le nord-ouest, alors que l'extrême-sud de la région est en phase de 0705-7199 (imprimé) submersion.
    [Show full text]
  • Deglacial Patterns and Ice-Sheet Dynamics in the Fjords of Southern Nordland, Norway
    NORWEGIAN JOURNAL OF GEOLOGY Vol 98 Nr. 4 https://dx.doi.org/10.17850/njg98-4-07 Deglacial patterns and ice-sheet dynamics in the fjords of southern Nordland, Norway Fredrik Høgaas1, Lars Olsen1, Lina Gislefoss1, Oddvar Longva1, Anders Romundset1 & Harald Sveian1 1Geological Survey of Norway, P.O. Box 6315 Torgarden, NO–7491 Trondheim, Norway. E-mail corresponding author (Fredrik Høgaas): [email protected] This paper presents results from glacial geomorphology mapping in and adjacent to Velfjorden and Ursfjorden in the southern Nordland region of Norway. Submarine and terrestrial landforms were studied and mapped using high-resolution multibeam bathymetric and airborne LiDAR data, in addition to reconnaissance in the field. The work unites ice-marginal deposits related to the established Tautra and Tjøtta glacial events which took place during the Younger Dryas (YD) chronozone. In Ursfjorden, an outlet glacier deposited a c. 100 m-high terminal moraine, whereas moraine ridges and a large sedimentary wedge were deposited in the inner part of Velfjorden. Highly elongated subglacial bedforms located inside the ice-marginal landforms reveal that the fjords were occupied by fast-flowing ice streams during YD. Eighteen new radiocarbon dates from the region, along with twelve recalibrated dates from previous studies, provide time-constraints for ice-sheet configuration and dynamics during deglaciation. Radiocarbon dates suggest that the outer coastal islands became ice-free prior to 14 cal ka BP. Glacially overridden shell-rich units dated to the Allerød Interstadial indicate that the YD ice sheet readvanced at least 5 km before depositing the terminal moraine in Ursfjorden. The ages of shells found near the distinct, regionally correlative, YD raised shoreline indicate that the glacial readvance culminated around early to mid-YD.
    [Show full text]
  • Pumice in the North Atlantic
    Ocean-transported pumice in the North Atlantic Anthony Newton PhD University of Edinburgh 1999 Declaration I, Anthony Newton hereby declare that the work contained herein is my own and has not previously been presented for examination. Any contributions by others is acknowledged in the text. September 1999 ii For Keith Newton 1930-1984 iii “Some days we would pass through pumice lying in ridges, each piece uniformly the size and appearance of a bath sponge, then again we should pass through perfect fields of small yellow pumice spread evenly over the surface just for all the world like a green field of grass covered all over with buttercups, and the undulation of the swell of the trade wind produced an indescribably pretty appearance.” (Reeves, 1884). iv Abstract The overall aims of this study are to identify the sources of the widespread Holocene pumice deposits found along the coasts of the North Atlantic region and establish the ages of the source eruptions. In order to tackle this, it is necessary to determine whether it is possible to “fingerprint” the pumice of individual eruptions and link ocean-transported material with the established tephrochronological framework based on the stratigraphy of airfall deposits. Over 1500 electron probe microanalyses and over 200 Secondary Ion Mass Spectrometry analyses have been undertaken on pumice and tephra samples. These are the first high quality grain specific analyses carried out on ocean-transported pumice in the North Atlantic. Current knowledge of the extent of pumice distribution in the North Atlantic region is assessed for both shoreline (natural) and archaeological contexts.
    [Show full text]
  • Geodiversity Audit & Action Plan for the Causeway Coast & Glens
    Geodiversity Audit & Action Plan for the Causeway Coast & Glens Region April 2013 William Burke Acknowledgements This document has been produced with the help of many individuals and organisations who have contributed to the process by offering advice, information, the use of their facilities and documents and invaluable comments on drafts. The authors are grateful to the following: Staff at the Causeway Coast and Glens Heritage Trust; Northern Ireland Environment Agency; Geological Survey NI; the National Trust; Queens University, Belfast; University of Ulster; Officers from Limavady, Coleraine, Ballymoney, Ballymena, Moyle and Larne District Councils, Western Education and Library Board, North Eastern Education and Library Board and for all the others who have contributed information and provided assistance. 1 TABLE OF CONTENTS 2 LIST OF FIGURES AND TABLES 4 PART 1 INTRODUCTION TO GEODIVERSITY 1.0 Introduction 1.1 Scope of the Report 6 1.2 Structure of the Report 6 1.3 Study area 7 1.4 Defining Geodiversity 8 1.5 The Relevance of Geodiversity 9 1.6 Conserving Earth Science in the CCGHT area – Strategic Considerations and Designations 10 1.6.1 Regional Development Strategy 10 1.6.2 Northern Area Plan 2016 10 1.6.3 Causeway Coast & Glens Tourism Masterplan 2004-2013 10 1.6.4 Causeway Coast & Glens Tourism Area Plan 11 1.6.5 Earth Science Conservation Review 11 1.6.6 Areas of Outstanding Natural Beauty 11 1.6.6.1 Antrim Coast and Glens AONB 12 1.6.6.2 Causeway Coast AONB 12 1.6.6.3 Binevenagh AONB 13 1.6.7 World Heritage Site Designation
    [Show full text]
  • Quaternary Sea Level Change in Scotland
    This is a repository copy of Quaternary sea level change in Scotland. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/124404/ Version: Accepted Version Article: Smith, DE, Barlow, NLM orcid.org/0000-0002-2713-2543, Bradley, SL et al. (4 more authors) (2019) Quaternary sea level change in Scotland. Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 110 (1-2). pp. 219-256. ISSN 1755-6910 https://doi.org/10.1017/S1755691017000469 (c) The Royal Society of Edinburgh 2018. This article has been published in a revised form in Earth and Environmental Science Transactions of The Royal Society of Edinburgh https://doi.org/10.1017/S1755691017000469 This version is free to view and download for private research and study only. Not for re-distribution, re-sale or use in derivative works. Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ Earth and Environmental Science Transactions of the Royal Society of Edinburgh Quaternary Sea Level Change Earth and Environmental Science Transactions of the Royal Society of Journal: Edinburgh Manuscript ID TRE-2016-0076.R1 Manuscript Type: The Quaternary o Scotland Date Submitted by the Author: n/a Complete List o Authors: Smith, David; ,niversity o O.
    [Show full text]
  • Moray and Caithness
    Moray and Caithness: A landscape fashioned by geology Moray and Caithness The far north-east of Scotland encompasses a wide range of landscapes, from the rolling hills of Moray and the coastal flagstone cliffs of Caithness, to the blanket peat bogs of the Flow Country and the ancient rugged A Landscape Fashioned by Geology mountains of eastern Sutherland. These landscapes have all formed during a long and complex geological Clive Auton, Jon Merritt and Kathryn Goodenough history, from rocks that were buckled and warped by continental collisions that occurred many hundreds of millions of years ago, to the sculpting of the hills and valleys by glaciers just a few thousand years ago. Since Neolithic times, the inhabitants of the region have made use of its geological resources and also changed its appearance irrevocably. This book describes the whole of that geological and human history, laying bare the events that have shaped the landscape of this remote but intriguing corner of Scotland. About the Authors Mor Clive Auton has worked as a field geologist in Scotland for almost thirty years on many aspects of the rocks and landscape, A particularly in the Highlands and Northern Isles, but also around the Moray and Solway firths. He is particularly interested in the y AN glacial history of Moray and Caithness and also in the Old Red Sandstone rocks of the Orcadian Basin. Clive is an active member D C of the Quaternary Research Association and has led many geological field excursions to the Caithness and Moray area. A Jon Merritt has worked as a field geologist on various aspects of the superficial deposits and glacial landforms of Scotland for over ith N thirty years, particularly in the Highlands and Islands.
    [Show full text]
  • Post Little Ice Age Rebound in the Glacier Bay Region
    Roman J. Motyka and others 57 Post Little Ice Age Rebound in the Glacier Bay Region Roman J. Motyka1,2, Christopher F. Larsen1, Jeffrey T. Freymueller1, and Keith A. Echelmeyer1 Abstract. Extreme uplift and sea level changes in southeast Alaska have been documented by (1) a regional GPS deformation array consisting of 74 sites; (2) 18 tide gage measurements of sea-level changes; and (3) 27 raised shoreline measurements of total uplift. The GPS data show peak uplift rates of 30 mm/ yr in Glacier Bay, and also delineated a second center of rapid uplift east of Yakutat with peak rates of 32 mm/yr. These studies documented rapid and continuous total sea level changes of up to 5.7 m, and constrained the age of the ongoing uplift to less than 250 yrs. The raised shorelines show a pattern of higher uplift surrounding the region of peak GPS uplift rates in Glacier Bay, while the dating of these shorelines shows that they began uplifting at the same time the massive Glacier Bay Icefield began its retreat. This is a direct observation of glacial isostatic rebound processes acting on timescales of only a few hundred years in southern Alaska. Introduction Icefields and glaciers in the coastal mountains of southern Alaska and Canada have undergone rapid thinning over the last 250 years (Arendt and others, 2002) and the associated unloading of the Earth’s surface has led to isostatic rebound of southern Alaska. In this study, we compared changes in sea level derived from tide gage observations and raised shoreline studies, and uplift rates derived from Global Positioning System (GPS) measurements to uplift predictions from viscoelastic rebound models.
    [Show full text]
  • Quaternary Sea Levels of the Brazilian Coast
    Quaternary ea Levels ofthe razilian Coast: by Kenitiro Suguio, Louis Martin and Jean-Marie Flexor Major contributions to the study of variations in sea level Factors Governing Changes in Sea Levels have come from recent work along the coast of Brazil, and Brazilian data were an important contribution to the recent Reconstructions of ancient sea levels represent relative and IGCP sea-level projects described in the last issue of not absolute positions, because relative sea-level changes Episodes by P.A. Pirazzoli. Several raised marine levels (Fig. 1) are the result of widespread variation of sea level have been recognized older than 123,000 yBP and associated (eustasy), and of variations in the elevation of continents. with older interglacials, but the most detailed chronology The latter are mainly controlled by horizontal or vertical concerns a series of raised shoreline features formed during tectonic movements over time scales ranging from long- the past 7,000 years. Certain differences from one coastal term to instantaneous (seismic), or by isostatic movements sector to another are attributed to variations of the geoid related to variations in the loading of land surfaces due to surface, or to local tectonics, and a detailed model for the the formation and disappearance of ice caps, the erosion of Holocene evolution of the central and southern Brazilian continents and accumulation of sediments in sedimentary coast is presented. (Ed.) basins, and transgressions and regressions on continental shelves (hyd ro-isostasy). Introduction G R AV I T Y, Until recent years, the ancient shorelines of regions such as CLIMATE EARTH MOVEMENTS ROTATION Brazil, then regarded as stable, were considered to be records of past global ocean levels One of the goals of the 4- 47 1 two IGCP projects (61 and 200) on sea levels was to deter- mine a worldwide eustatic curve for the Holocene (see volume changes volume changes distri bution Firazzoli, 1988).
    [Show full text]
  • Larsen C 2003.Pdf
    Rapid Uplift Of Southern Alaska Caused By Recent Ice Loss Item Type Thesis Authors Larsen, Christopher Fairlamb Download date 25/09/2021 02:17:36 Link to Item http://hdl.handle.net/11122/8659 INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy subm itted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand comer and continuing from left to right in equal sections with small overlaps. ProQuest Information and Learning 300 North Zeeb Road, Ann Arbor, Ml 48106-1346 USA 800-521-0600 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. RAPID UPLIFT OF SOUTHERN ALASKA CAUSED BY RECENT ICE LOSS A THESIS Presented to the Faculty of the University of Alaska Fairbanks in partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY By Christopher Fairlamb Larsen, B.S., M.S, Fairbanks, Alaska May 2003 Reproduced with permission of the copyright owner.
    [Show full text]
  • Hamilton West Harbour Shoreline & Breakwater
    Hamilton West Harbour Shoreline & Breakwater Class Environmental Assessment Environmental Study Report Prepared by Dillon Consulting Limited 11-5710 April 17th, 2013 Hamilton West Harbour Shoreline and Breakwater Class Environmental Assessment: Environmental Study Report, April 17, 2013 TABLE OF CONTENTS Page EXECUTIVE SUMMARY ......................................................................................................... i 1.0 INTRODUCTION ...............................................................................................................1 2.0 BACKGROUND .................................................................................................................2 3.0 STUDY APPROACH ..........................................................................................................8 3.1. Evaluation Criteria ...............................................................................................................9 4.0 EXISTING CONDITIONS ................................................................................................10 4.1. Natural Environment ..........................................................................................................10 4.2. Public Access, Parks and Open Space ...............................................................................14 4.2.1. Public Access .........................................................................................................14 4.2.2. Parks and Open Space Areas .................................................................................15
    [Show full text]